灵山岛下白垩统软沉积物变形构造类型划分及其地质意义
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摘要
软沉积物变形构造是沉积物沉积之后、固结成岩之前尚处于塑性状态时,在液化作用和各种驱动力作用下发生不同程度变形的一系列构造。灵山岛下白垩统发育有多尺度、多形态、多层位、多期次、多成因的软沉积物变形构造。为研究其具体类型和成因机理,以形态特征为基础,以驱动力为分类依据,将灵山岛下白垩统软沉积物变形构造划分为斜坡上的重力驱动、密度倒置条件下的重力驱动和孔隙流体作用下的剪切力驱动等三种类型。此外,结合灵山岛下白垩统滑塌体内部的软沉积物变形构造分布特征,根据斜坡上重力驱动的软沉积物变形构造形成时所遭受的应力类型,将其进一步分为挤压型、拉伸型和剪切型等三个亚类。在分析研究灵山岛软沉积物变形构造的基本类型、发育情况和分布特征等基础上,认为灵山岛早白垩世地震活动非常频繁。驱动力直接作用于软沉积物,驱动力的种类、大小、作用方式和持续时间是影响软沉积物变形构造类型、形态和规模的重要因素,因此,从驱动力角度对其进行系统划分具有科学性、适用性和可行性。探讨软沉积物变形构造的分类方案对其野外识别和成因分析具有科学价值。
Soft-sediment deformation structures( SSDS) are a series of structures formed due to transformation of plastic sediment under liquidization and various driving forces after deposition but before lithification. SSDS are often developed in the strata with different scales,shapes,periods and origins. No doubt that earthquake is one of the most common causes of deformation of soft sediments,however,it is not limited only to earthquakes. SSDS are not a diagnosis of any specific trigger mechanism. According to the classification scheme of induced events,it is much more applicable in the same event,but it is difficult to distinguish the real cause in " multi causes and even the same phenomenon" of deformation. Therefore,the classification based on origin is often limited. In fact,the driving forces are the most direct factors causing the deformation of soft sediments and directly control specific forms of deforming structures.In order to clarify their specific types and development,this study advocates the classification of SSDS according to different driving forces. Based on literature and field outcrop investigation,the Early Cretaceous gravity flows deposit in the Lingshan Island are developed very well with SSDS in multi scales,forms,layers,periods and genesises,which can be classified into three types: the SSDS driven by gravity acting on slopes; the SSDS driven by gravity due to a reverse density gradient; and the SSDS driven by upward shear due to pore fluid. In addition,considering the SSDS development in the interior of the lower Cretaceous slump in the Lingshan island,according to the types of stresses when the deformation structures were formed,SSDS driven by gravity acting on slopes are further divided into three subtypes: compression types,tension types and shear types. 3 categories of more than 10 kinds of SSDS are identified in the Lower Cretaceous in Lingshan Island: SSDS driven by gravity acting on slopes including compression types( synsedimentary reverse faults and disordered compression deformation structures etc.),tension types( synsedimentary boudins,step faults and domino structures etc.) and shear types( some folds and fractures caused by shear and soft double structures etc.); SSDS driven by gravity due to a reverse density gradient including load structures,flame structures and ball-and-pillow structures etc.; SSDS driven by upward shear due to pore fluid including liquefied diaper,water-escape structures,convolute lamination and sandstone dykes etc. According to the types,development and distributions of SSDS,Early Cretaceous seismic activity was very frequent in Lingshan Island. The driving forces directly act on the soft sediment. And their types,strength,modes of action and duration affect the types,shapes and scales of the SSDS. Classification of soft-sediment deformation structures based on driving forces of Lower Cretaceous in Lingshan Island can distinguish SSDS in the slump beds from the normal sedimentary layer,and can distinguish SSDS formed during the slump process from the earthquake process. This classification can clarifies the dynamic mechanism of the deformation of soft sediment. Hence it is scientific,applicative and feasible to divide SSDS based on the driving forces. Discussion on classification of SSDS is benefit to facilitate its field identification and genesis analysis,and to provide a theoretical basis for other similar geological researches.
Soft-sediment deformation structures( SSDS) are a series of structures formed due to transformation of plastic sediment under liquidization and various driving forces after deposition but before lithification. SSDS are often developed in the strata with different scales,shapes,periods and origins. No doubt that earthquake is one of the most common causes of deformation of soft sediments,however,it is not limited only to earthquakes. SSDS are not a diagnosis of any specific trigger mechanism. According to the classification scheme of induced events,it is much more applicable in the same event,but it is difficult to distinguish the real cause in " multi causes and even the same phenomenon" of deformation. Therefore,the classification based on origin is often limited. In fact,the driving forces are the most direct factors causing the deformation of soft sediments and directly control specific forms of deforming structures.In order to clarify their specific types and development,this study advocates the classification of SSDS according to different driving forces. Based on literature and field outcrop investigation,the Early Cretaceous gravity flows deposit in the Lingshan Island are developed very well with SSDS in multi scales,forms,layers,periods and genesises,which can be classified into three types: the SSDS driven by gravity acting on slopes; the SSDS driven by gravity due to a reverse density gradient; and the SSDS driven by upward shear due to pore fluid. In addition,considering the SSDS development in the interior of the lower Cretaceous slump in the Lingshan island,according to the types of stresses when the deformation structures were formed,SSDS driven by gravity acting on slopes are further divided into three subtypes: compression types,tension types and shear types. 3 categories of more than 10 kinds of SSDS are identified in the Lower Cretaceous in Lingshan Island: SSDS driven by gravity acting on slopes including compression types( synsedimentary reverse faults and disordered compression deformation structures etc.),tension types( synsedimentary boudins,step faults and domino structures etc.) and shear types( some folds and fractures caused by shear and soft double structures etc.); SSDS driven by gravity due to a reverse density gradient including load structures,flame structures and ball-and-pillow structures etc.; SSDS driven by upward shear due to pore fluid including liquefied diaper,water-escape structures,convolute lamination and sandstone dykes etc. According to the types,development and distributions of SSDS,Early Cretaceous seismic activity was very frequent in Lingshan Island. The driving forces directly act on the soft sediment. And their types,strength,modes of action and duration affect the types,shapes and scales of the SSDS. Classification of soft-sediment deformation structures based on driving forces of Lower Cretaceous in Lingshan Island can distinguish SSDS in the slump beds from the normal sedimentary layer,and can distinguish SSDS formed during the slump process from the earthquake process. This classification can clarifies the dynamic mechanism of the deformation of soft sediment. Hence it is scientific,applicative and feasible to divide SSDS based on the driving forces. Discussion on classification of SSDS is benefit to facilitate its field identification and genesis analysis,and to provide a theoretical basis for other similar geological researches.
引文
[1] Selley R C. An introduction to sedimentology[M]. London and New York:Academic Press,1982:233-238.
[2]赵澂林,刘孟慧.湖相沉积岩中的同生变形构造及其地质意义[J].岩石学报,1988,4(4):149-155.[Zhao Chenglin,Liu Menghui. Contemporaneous deformed structures in lacustring sedimentary rocks and their geological significance[J]. Acta Petrologica Sinica,1988,4(4):149-155.]
[3] van Loon A J. Soft-sediment deformations in the Kleszczów Graben(central Poland)[J]. Sedimentary Geology,2002,147(1/2):57-70.
[4] van Loon A J. Soft-sediment deformation structures in siliciclastic sediments:an overview[J]. Geologos,2009,15(1):3-55.
[5] Moretti M,Sabato L. Recognition of trigger mechanisms for soft-sediment deformation in the Pleistocene lacustrine deposits of the Sant’Arcangelo Basin(Southern Italy):seismic shock vs. overloading[J]. Sedimentary Geology,2007,196(1/2/3/4):31-45.
[6] Oliveira C M M,Hodgson D M,Flint S S. Aseismic controls on in situ soft-sediment deformation processes and products in submarine slope deposits of the Karoo Basin,South Africa[J]. Sedimentology,2009,56(5):1201-1225.
[7] Owen G,Moretti M. Identifying triggers for liquefaction-induced soft-sediment deformation in sands[J]. Sedimentary Geology,2011,235(3/4):141-147.
[8]杜远生,韩欣.论震积作用和震积岩[J].地球科学进展,2000,15(4):389-394.[Du Yuansheng,Han Xin. Seismo-deposition and seismites[J]. Advance in Earth Sciences,2000,15(4):389-394.]
[9] Moretti M,Pieri P,Tropeano M. Late Pleistocene soft-sediment deformation structures interpreted as seismites in paralic deposits in the city of Bari(Apulian foreland,southern Italy)[M]//Ettensohn F R,Rast N,Brett C E. Ancient seismites,Special Paper 359. Boulder,CO:Geological Society of America,2002:75-85.
[10] Mazumder R,van Loon A J,Arima M. Soft-sediment deformation structures in the Earth’s oldest seismites[J]. Sedimentary Geology,2006,186(1/2):19-26.
[11]杜远生,SHI G,龚一鸣,等.东澳大利亚南悉尼盆地二叠系与地震沉积有关的软沉积变形构造[J].地质学报,2007,81(4):511-518.[Du Yuansheng,SHI G,Gong Yiming,et al. Permian soft-sediment deformation structures related to earthquake in the southern Sydney Basin,eastern Australia[J]. Acta Geologica Sinica,2007,81(4):511-518.]
[12] Montenat C,Barrier P,d'Estevou P O,et al. Seismites:an attempt at critical analysis and classification[J]. Sedimentary Geology,2007,196(1/2/3/4):5-30.
[13]乔秀夫,李海兵.沉积物的地震及古地震效应[J].古地理学报,2009,11(6):593-610.[Qiao Xiufu,Li Haibing. Effect of earthquake and ancient earthquake on sediments[J]. Journal of Palaeogeography,2009,11(6):593-610.]
[14]杜远生.中国地震事件沉积研究的若干问题探讨[J].古地理学报,2011,13(6):581-590.[Du Yuansheng. Discussion about studies of earthquake event deposit in China[J]. Journal of Palaeogeography,2011,13(6):581-590.]
[15]乔秀夫,郭宪璞.新疆西南天山下侏罗统软沉积物变形研究[J].地质论评,2011,57(6):761-769.[Qiao Xiufu,Guo Xianpu. On the lower Jurassic soft-sediment deformation of southwestern Tianshan Mountains,Xinjiang,China[J]. Geological Review,2011,57(6):761-769.]
[16] van Loon A J,Pisarska-Jamro6)zy M,Narti2s M,et al. Seismites resulting from high-frequency,high-magnitude earthquakes in Latvia caused by Late Glacial glacio-isostatic uplift[J]. Journal of Palaeogeography,2016,5(4):363-380.
[17] Alfaro P,Delgado J,Estévez A,et al. Liquefaction and fluidization structures in Messinian storm deposits(Bajo Segura Basin,Betic Cordillera,southern Spain)[J]. International Journal of Earth Sciences,2002,91(3):505-513.
[18] Chen J T,Chough S K,Chun S S,et al. Limestone pseudoconglomerates in the Late Cambrian Gushan and Chaomidian Formations(Shandong Province,China):soft-sediment deformation induced by storm-wave loading[J]. Sedimentology,2009,56(4):1174-1195.
[19] Dawson A G. Linking tsunami deposits,submarine slides and offshore earthquakes[J]. Quaternary International,1999,60(1):119-126.
[20] Matsumoto D,Naruse H,Fujino S,et al. Truncated flame structures within a deposit of the Indian Ocean Tsunami:evidence of syn-sedimentary deformation[J]. Sedimentology,2008,55(6):1559-1570.
[21] Meshram D C,Sangode S J,Gujar A R,et al. Occurrence of soft sediment deformation at Dive Agar beach,west coast of India:possible record of the Indian Ocean tsunami(2004)[J]. Natural Hazards,2011,57(2):385-393.
[22]吕洪波,王俊,张海春.山东灵山岛晚中生代滑塌沉积层的发现及区域构造意义初探[J].地质学报,2011,85(6):938-946.[LüHongbo,Wang Jun,Zhang Haichun. Discovery of the Late Mesozoic slump beds in Lingshan Island,Shandong,and a pilot research on the regional tectonics[J]. Acta Geologica Sinica,2011,85(6):938-946.]
[23]吕洪波,张海春,王俊,等.灵山岛早白垩世复理石不是陆内三角洲沉积:答钟建华教授[J].地质论评,2013,59(1):11-14.[LüHongbo,Zhang Haichun,Wang Jun,et al. The Early Cretaceous Flysch found in the Lingshan Island:not deltaic deposits on land:A reply to the argument from Professor ZHONG Jianhua[J].Geological Review,2013,59(1):11-14.]
[24]王安东,周瑶琪,闫华,等.山东省灵山岛早白垩世软沉积物变形构造特征[J].古地理学报,2013,15(5):717-728.[Wang Andong,Zhou Yaoqi,Yan Hua,et al. Characteristics of soft-sediment deformation structures of the Early Cretaceous in Lingshan Island of Shandong province[J]. Journal of Palaeogeography,2013,15(5):717-728.]
[25] Alves T M. Submarine slide blocks and associated soft-sediment deformation in deep-water basins:a review[J]. Marine and Petroleum Geology,2015,67:262-285.
[26]葛毓柱,钟建华,樊晓芳,等.山东灵山岛滑塌体内部沉积及构造特征研究[J].地质论评,2015,61(3):634-644.[Ge Yuzhu,Zhong Jianhua,Fan Xiaofang,et al. Study on internal sedimentary and structural features of the slump body in Lingshan Island,Qingdao,Shandong[J]. Geological Review,2015,61(3):634-644.]
[27]杜远生,彭冰霞,韩欣.广西北海涠洲岛晚更新世火山活动引起的地震同沉积变形构造[J].沉积学报,2005,23(2):203-209.[Du Yuansheng,Peng Bingxia,Han Xin. Syn-depositional deformation structures by earthquake related to volcanic activity of the Late Pleistocene in Weizhou Island,Beihai city,Guangxi[J].Acta Sedimentologica Sinica,2005,23(2):203-209.]
[28] Harris C,Murton J,Davies M C R. Soft-sediment deformation during thawing of ice-rich frozen soils:results of scaled centrifuge modelling experiments[J]. Sedimentology,2000,47(3):687-700.
[29]钟建华,王冠民,王夕宾,等.黄河下游冰成滑塌与塌陷构造的研究[J].沉积学报,2002,20(2):261-266.[Zhong Jianhua,Wang Guanmin,Wang Xibin,et al. Study on the ice-induced slump and subsidence structures in the lower course of Yellow River[J]. Acta Sedimentologica Sinica,2002,20(2):261-266.]
[30] Weaver L,Arnaud E. Polyphase glacigenic deformation in the Waterloo Moraine,Kitchener,Ontario,Canada[J]. Sedimentary Geology,2011,235(3/4):292-303.
[31] Moretti M,Soria J M,Alfaro P,et al. Asymmetrical soft-sediment deformation structures triggered by rapid sedimentation in turbiditic deposits(Late Miocene,Guadix Basin,Southern Spain)[J]. Facies,2001,44(1):283-294.
[32] P7ldsaar K,Ainsaar L. Extensive soft-sediment deformation structures in the early Darriwilian(Middle Ordovician)shallow marine siliciclastic sediments formed on the Baltoscandian carbonate ramp,northwestern Estonia[J]. Marine Geology,2014,356:111-127.
[33]刘金华,吴立峰,乔力,等.苏北盆地高邮凹陷深凹带古近系戴南组软沉积物变形构造及沉积模式研究[J].地质论评,2014,60(5):1019-1025.[Liu Jinhua,Wu Lifeng,Qiao Li,et al. Depositional model and characteristic of soft-sediment deformation structures of the Paleogene Dainan Formation in Gaoyou sag,North Jiangsu Basin[J]. Geological Review,2014,60(5):1019-1025.]
[34]杜远生,余文超.地震和非地震引发的软沉积物变形[J].古地理学报,2017,19(1):65-72.[Du Yuansheng,Yu Wenchao.Earthquake-caused and non-earthquake-caused soft-sediment deformations[J]. Journal of Palaeogeography,2017,19(1):65-72.]
[35]山穆玕,著.冯增昭,刘敏,译.地震岩问题[J].古地理学报,2017,19(1):19-64.[Shanmugam G. Feng Zengzhao,Liu Min,Trans. The seismite problem[J]. Journal of Palaeogeography,2017,19(1):19-64.]
[36] Owen G,Moretti M,Alfaro P. Recognising triggers for soft-sediment deformation:current understanding and future directions[J].Sedimentary Geology,2011,235(3/4):133-140.
[37] Shanmugam G. Global case studies of soft-sediment deformation structures(SSDS):definitions,classifications,advances,origins,and problems[J]. Journal of Palaeogeography,2017,6(4):251-320.
[38] Seilacher A. Fault-graded beds interpreted as seismites[J]. Sedimentology,1969,13(1/2):155-159.
[39] Owen G. Experimental soft-sediment deformation:structures formed by the liquefaction of unconsolidated sands and some ancient examples[J]. Sedimentology,1996,43(2):279-293.
[40]冯先岳.地震振动液化形变的研究[J].内陆地震,1989,3(4):299-307.[Feng Xianyue. Study on the deformation caused by seismic vibrational liquefaction[J]. Inland Earthquake,1989,3(4):299-307.]
[41] Moretti M,Alfaro P,Caselles O,et al. Modelling seismites with a digital shaking table[J]. Tectonophysics,1999,304(4):369-383.
[42]鄢继华,崔永北,陈世悦.几种常见震积岩相标志在模拟实验中的识别[J].沉积学报,2009,27(6):1131-1137.[Yan Jihua,Cui Yongbei,Chen Shiyue. Identification of common facies indicators of seismites in simulated experiments[J]. Acta Sedimentologica Sinica,2009,27(6):1131-1137.]
[43]张斌,王萍,王建存.岷江上游堰塞湖沉积中软沉积物变形构造成因讨论[J].地震研究,2011,34(1):67-74.[Zhang Bin,Wang Ping,Wang Jiancun. Discussion of the origin of the soft-sediment deformation structures in Paleo-dammed Lake sediments in the upper reaches of the Minjiang River[J]. Journal of Seismological Research,2011,34(1):67-74.]
[44]冯增昭,鲍志东,郑秀娟,等.中国软沉积物变形构造及地震岩研究简评[J].古地理学报,2017,19(1):7-12.[Feng Zengzhao,Bao Zhidong,Zheng Xiujuan,et al. Researches of soft-sediment deformation structures and seismites in China:a brief review[J]. Journal of Palaeogeography,2017,19(1):7-12.]
[45]冯增昭.一次成功的专题研讨会:“多成因的软沉积物变形构造及地震岩”[J].古地理学报,2017,19(1):1-6.[Feng Zengzhao. A successful symposium of“Multi-origin of soft-sediment deformation structures and seismites”[J]. Journal of Palaeogeography,2017,19(1):1-6.]
[46]李勇,钟建华,邵珠福,等.软沉积变形构造的分类和形成机制研究[J].地质论评,2012,58(5):829-838.[Li Yong,Zhong Jianhua,Shao Zhufu,et al. An overview on the classification and genesis of soft-sediment deformation structure[J]. Geological Review,2012,58(5):829-838.]
[47]栾光忠,李安龙,王建,等.青岛主要海岛成因分类及其地质环境分析[J].中国海洋大学学报,2010,40(8):111-116.[Luan Guangzhong,Li Anlong,Wang Jian,et al. The geological origin division of the main sea island in Qingdao area and environment analysis[J]. Periodical of Ocean University of China,2010,40(8):111-116.]
[48]山东省第四地质矿产勘察院.山东省区域地质[M].济南:山东省地图出版社,2003:1-970.[Shandong Province NO. 4 Institute of Geological and Mineral Survey. Regional geology of Shandong province[M]. Jinan:Shandong Cartographic Press,2013:1-970.]
[49]吕洪波,张海春,王俊,等.山东胶南灵山岛晚中生代浊积岩中发现巨大滑积岩块[J].地质论评,2012,58(1):80-81.[LüHongbo,Zhang Haichun,Wang Jun,et al. The huge slide block is found in Late Mesozoic turbidite in Lingshan Island, Jiaonan,Shandong[J]. Geological Review,2012,58(1):80-81.]
[50]张海春,吕洪波,李建国,等.山东青岛早白垩世新地层单位—灵山岛组[J].地层学杂志,2013,37(2):216-222.[Zhang Haichun,LüHongbo,Li Jianguo,et al. The Lingshandao Formation:a new lithostratigraphic unit of the Early Cretaceous in Qingdao,Shandong,China[J]. Journal of Stratigraphy,2013,37(2):216-222.]
[51]周瑶琪,张振凯,梁文栋,等.山东东部晚中生代构造—岩浆活动及原型盆地恢复[J].地学前缘,2015,22(1):137-156.[Zhou Yaoqi,Zhang Zhenkai,Liang Wendong,et al. Late Mesozoic tectono-magmatic activities and prototype basin restoration in eastern Shandong province,China[J]. Earth Science Frontiers,2015,22(1):137-156.]
[52] Alsop G I,Marco S. Soft-sediment deformation within seismogenic slumps of the Dead Sea Basin[J]. Journal of Structural Geology,2011,33(4):433-457.
[53]董晓朋,吕洪波,张星,等.山东灵山岛早白垩世复理石软沉积物变形期次解析[J].地质论评,2013,59(6):1060-1067.[Dong Xiaopeng,LüHongbo,Zhang Xing,et al. Stage analysis on the soft-sediment deformation in the Early Cretaceous Flysch,Lingshan Island, Shandong province[J]. Geological Review,2013,59(6):1060-1067.]
[54] van Loon A J,Wiggers A J. Metasedimentary“graben”and associated structures in the lagoonal Almere Member(Groningen Formation,The Netherlands)[J]. Sedimentary Geology,1976,16(4):237-254.
[55]张邦花,田洪水,张增奇,等.地质名山馒头山及其附近早寒武世古地震沉积事件研究[J].沉积学报,2012,30(6):1021-1031.[Zhang Banghua,Tian Hongshui,Zhang Zengqi,et al. Paleoseismic depositional events of the famous geological mountainMantoushan and its vicinity in the Early Cambrian[J]. Acta Sedimentologica Sinica,2012,30(6):1021-1031.]
[56] Yang R C,Van Loon A J. Early Cretaceous slumps and turbidites with peculiar soft-sediment deformation structures on Lingshan Island(Qingdao,China)indicating a tensional tectonic regime[J].Journal of Asian Earth Sciences,2016,129:206-219.
[57]杜芳鹏,刘池洋,王建强,等.鄂尔多斯盆地南部上三叠统延长组软沉积变形特征及构造意义[J].现代地质,2014,28(2):314-320.[Du Fangpeng,Liu Chiyang,Wang Jianqiang,et al.Characteristics and tectonic sense of soft sedimentary structures in Yanchang Formation,South Ordos Basin[J]. Geoscience,2014,28(2):314-320.]
[58]邵珠福,钟建华,李勇,等.青岛灵山岛晚中生代重力流沉积特征及环境分析[J].地质论评,2014,60(3):555-566.[Shao Zhufu,Zhong Jianhua,Li Yong,et al. The sedimentary characteristics and environmental analysis of Late Mesozoic gravity flows in Lingshan Island[J]. Geological Review,2014,60(3):555-566.]
[59]张传恒,刘典波,张传林,等.新疆博格达地区早二叠世软沉积物变形构造:弧后碰撞前陆盆地地震记录[J].地学前缘,2006,13(4):255-266.[Zhang Chuanheng,Liu Dianbo,Zhang Chuanlin,et al. Early Permian seismically induced soft-sediment deformational structures in Bogda region,Xinjiang:stratigraphic records of earthquakes in the retroarc collisional foreland basin[J].Earth Science Frontiers,2006,13(4):255-266.]
[60]钟建华,倪良田,邵珠福,等.几种较特殊的地震成因软变形沉积构造[J].地质科学,2015,50(3):665-683.[Zhong Jianhua,Ni Liangtian,Shao Zhufu,et al. Study on several special sedimentary structures of earthquake-induced soft deformations[J]. Chinese Journal of Geology,2015,50(3):665-683.]
[61] Owen G. Load structures:gravity-driven sediment mobilization in the shallow subsurface[J]. Geological Society,London,Special Publications,2003,216(1):21-34.
[62]乔秀夫,李海兵.枕、球—枕构造:地层中的古地震记录[J].地质论评,2008,54(6):721-730.[Qiao Xiufu,Li Haibing. Pillow,ball-and-pillow structures:paleo-seismic records within strata[J].Geological Review,2008,54(6):721-730.]
[63] Yamamoto Y. Dewatering structure and soft-sediment deformation controlled by slope instability:examples from the Late Miocene to Pliocene Miura-Boso accretionary prism and trench-slope basin,central Japan[J]. Marine Geology,2014,356:65-70.
[64]杨剑萍,聂玲玲,杨君.柴达木盆地西南缘新近系与地震沉积有关的软沉积物变形构造及其地质意义[J].沉积学报,2008,26(6):967-974.[Yang Jianping,Nie Lingling,Yang Jun. Softsediment deformation structures of Neogene related to earthquake and its geological significance in the southwestern margin of Qaidam Basin[J]. Acta Sedimentologica Sinica,2008,26(6):967-974.]
[65] Finkl Jr C W. Sedimentary structures—their character and physical basis:J.R.L. Allen,1982. Vols. I,II. Developments in Sedimentology,30A and 30B. Elsevier,Amsterdam,Vol. I:xvii+593pp.,US$98.00,Dfl.245.00; Vol. II:xiii+663 pp.,US$104.00,Dfl.260.00[J]. Earth-Science Reviews,1983,19(4):362-363.
[66]周瑶琪,张振凯,许红,等.灵山岛沉积物软变形构造特征[J].海洋地质前沿,2015,31(4):42-54.[Zhou Yaoqi,Zhang Zhenkai,Xu Hong,et al. Soft-sediment deformation structures in the sediments at Lingshan Island[J]. Marine Geology Frontiers,2015,31(4):42-54.]
[67] Simms M J. Uniquely extensive soft-sediment deformation in the Rhaetian of the UK:evidence for earthquake or impact?[J].Palaeogeography,Palaeoclimatology, Palaeoecology,2007,244(1/2/3/4):407-423.
[68]乔秀夫,宋天锐,高林志,等.碳酸盐岩振动液化地震序列[J].地质学报,1994,68(1):16-34.[Qiao Xiufu,Song Tianrui,Gao Linzhi,et al. Seismic sequence in carbonate rocks by vibrational liquefaction[J]. Acta Geologica Sinica,1994,68(1):16-34.]
[69]钟建华,梁刚.沉积构造的研究现状及发展趋势[J].地质论评,2009,55(6):831-839.[Zhong Jianhua,Liang Gang. Situation of study and development tendency of sedimentary structure[J].Geological Review,2009,55(6):831-839.]
[70] Mc Laughlin P I,Brett C E. Eustatic and tectonic control on the distribution of marine seismites:examples from the Upper Ordovician of Kentucky,USA[J]. Sedimentary Geology,2004,168(3/4):165-192.
[71] Rossetti D F,Santos Jr A E. Events of sediment deformation and mass failure in Upper Cretaceous estuarine deposits(CametáBasin,northern Brazil)as evidence for seismic activity[J]. Sedimentary Geology,2003,161(1/2):107-130.
[72]周勇,纪友亮,万璐,等.山东省胶莱盆地东北部下白垩统莱阳组震积岩特征及地质意义[J].古地理学报,2011,13(5):517-528.[Zhou Yong,Ji Youliang,Wan Lu,et al. Characteristics and geologic significance of seismites in the Lower Cretaceous Laiyang Formation in northeastern Jiaolai Basin in Shandong province[J].Journal of Palaeogeography,2011,13(5):517-528.]
[73]刘颖,谢君斐.砂土震动液化[M].北京:地震出版社,1984:1-255.[Liu Ying,Xie Junfei. Sand vibration liquefaction[M]. Beijing:Seismological Press,1984:1-255.]
[2]赵澂林,刘孟慧.湖相沉积岩中的同生变形构造及其地质意义[J].岩石学报,1988,4(4):149-155.[Zhao Chenglin,Liu Menghui. Contemporaneous deformed structures in lacustring sedimentary rocks and their geological significance[J]. Acta Petrologica Sinica,1988,4(4):149-155.]
[3] van Loon A J. Soft-sediment deformations in the Kleszczów Graben(central Poland)[J]. Sedimentary Geology,2002,147(1/2):57-70.
[4] van Loon A J. Soft-sediment deformation structures in siliciclastic sediments:an overview[J]. Geologos,2009,15(1):3-55.
[5] Moretti M,Sabato L. Recognition of trigger mechanisms for soft-sediment deformation in the Pleistocene lacustrine deposits of the Sant’Arcangelo Basin(Southern Italy):seismic shock vs. overloading[J]. Sedimentary Geology,2007,196(1/2/3/4):31-45.
[6] Oliveira C M M,Hodgson D M,Flint S S. Aseismic controls on in situ soft-sediment deformation processes and products in submarine slope deposits of the Karoo Basin,South Africa[J]. Sedimentology,2009,56(5):1201-1225.
[7] Owen G,Moretti M. Identifying triggers for liquefaction-induced soft-sediment deformation in sands[J]. Sedimentary Geology,2011,235(3/4):141-147.
[8]杜远生,韩欣.论震积作用和震积岩[J].地球科学进展,2000,15(4):389-394.[Du Yuansheng,Han Xin. Seismo-deposition and seismites[J]. Advance in Earth Sciences,2000,15(4):389-394.]
[9] Moretti M,Pieri P,Tropeano M. Late Pleistocene soft-sediment deformation structures interpreted as seismites in paralic deposits in the city of Bari(Apulian foreland,southern Italy)[M]//Ettensohn F R,Rast N,Brett C E. Ancient seismites,Special Paper 359. Boulder,CO:Geological Society of America,2002:75-85.
[10] Mazumder R,van Loon A J,Arima M. Soft-sediment deformation structures in the Earth’s oldest seismites[J]. Sedimentary Geology,2006,186(1/2):19-26.
[11]杜远生,SHI G,龚一鸣,等.东澳大利亚南悉尼盆地二叠系与地震沉积有关的软沉积变形构造[J].地质学报,2007,81(4):511-518.[Du Yuansheng,SHI G,Gong Yiming,et al. Permian soft-sediment deformation structures related to earthquake in the southern Sydney Basin,eastern Australia[J]. Acta Geologica Sinica,2007,81(4):511-518.]
[12] Montenat C,Barrier P,d'Estevou P O,et al. Seismites:an attempt at critical analysis and classification[J]. Sedimentary Geology,2007,196(1/2/3/4):5-30.
[13]乔秀夫,李海兵.沉积物的地震及古地震效应[J].古地理学报,2009,11(6):593-610.[Qiao Xiufu,Li Haibing. Effect of earthquake and ancient earthquake on sediments[J]. Journal of Palaeogeography,2009,11(6):593-610.]
[14]杜远生.中国地震事件沉积研究的若干问题探讨[J].古地理学报,2011,13(6):581-590.[Du Yuansheng. Discussion about studies of earthquake event deposit in China[J]. Journal of Palaeogeography,2011,13(6):581-590.]
[15]乔秀夫,郭宪璞.新疆西南天山下侏罗统软沉积物变形研究[J].地质论评,2011,57(6):761-769.[Qiao Xiufu,Guo Xianpu. On the lower Jurassic soft-sediment deformation of southwestern Tianshan Mountains,Xinjiang,China[J]. Geological Review,2011,57(6):761-769.]
[16] van Loon A J,Pisarska-Jamro6)zy M,Narti2s M,et al. Seismites resulting from high-frequency,high-magnitude earthquakes in Latvia caused by Late Glacial glacio-isostatic uplift[J]. Journal of Palaeogeography,2016,5(4):363-380.
[17] Alfaro P,Delgado J,Estévez A,et al. Liquefaction and fluidization structures in Messinian storm deposits(Bajo Segura Basin,Betic Cordillera,southern Spain)[J]. International Journal of Earth Sciences,2002,91(3):505-513.
[18] Chen J T,Chough S K,Chun S S,et al. Limestone pseudoconglomerates in the Late Cambrian Gushan and Chaomidian Formations(Shandong Province,China):soft-sediment deformation induced by storm-wave loading[J]. Sedimentology,2009,56(4):1174-1195.
[19] Dawson A G. Linking tsunami deposits,submarine slides and offshore earthquakes[J]. Quaternary International,1999,60(1):119-126.
[20] Matsumoto D,Naruse H,Fujino S,et al. Truncated flame structures within a deposit of the Indian Ocean Tsunami:evidence of syn-sedimentary deformation[J]. Sedimentology,2008,55(6):1559-1570.
[21] Meshram D C,Sangode S J,Gujar A R,et al. Occurrence of soft sediment deformation at Dive Agar beach,west coast of India:possible record of the Indian Ocean tsunami(2004)[J]. Natural Hazards,2011,57(2):385-393.
[22]吕洪波,王俊,张海春.山东灵山岛晚中生代滑塌沉积层的发现及区域构造意义初探[J].地质学报,2011,85(6):938-946.[LüHongbo,Wang Jun,Zhang Haichun. Discovery of the Late Mesozoic slump beds in Lingshan Island,Shandong,and a pilot research on the regional tectonics[J]. Acta Geologica Sinica,2011,85(6):938-946.]
[23]吕洪波,张海春,王俊,等.灵山岛早白垩世复理石不是陆内三角洲沉积:答钟建华教授[J].地质论评,2013,59(1):11-14.[LüHongbo,Zhang Haichun,Wang Jun,et al. The Early Cretaceous Flysch found in the Lingshan Island:not deltaic deposits on land:A reply to the argument from Professor ZHONG Jianhua[J].Geological Review,2013,59(1):11-14.]
[24]王安东,周瑶琪,闫华,等.山东省灵山岛早白垩世软沉积物变形构造特征[J].古地理学报,2013,15(5):717-728.[Wang Andong,Zhou Yaoqi,Yan Hua,et al. Characteristics of soft-sediment deformation structures of the Early Cretaceous in Lingshan Island of Shandong province[J]. Journal of Palaeogeography,2013,15(5):717-728.]
[25] Alves T M. Submarine slide blocks and associated soft-sediment deformation in deep-water basins:a review[J]. Marine and Petroleum Geology,2015,67:262-285.
[26]葛毓柱,钟建华,樊晓芳,等.山东灵山岛滑塌体内部沉积及构造特征研究[J].地质论评,2015,61(3):634-644.[Ge Yuzhu,Zhong Jianhua,Fan Xiaofang,et al. Study on internal sedimentary and structural features of the slump body in Lingshan Island,Qingdao,Shandong[J]. Geological Review,2015,61(3):634-644.]
[27]杜远生,彭冰霞,韩欣.广西北海涠洲岛晚更新世火山活动引起的地震同沉积变形构造[J].沉积学报,2005,23(2):203-209.[Du Yuansheng,Peng Bingxia,Han Xin. Syn-depositional deformation structures by earthquake related to volcanic activity of the Late Pleistocene in Weizhou Island,Beihai city,Guangxi[J].Acta Sedimentologica Sinica,2005,23(2):203-209.]
[28] Harris C,Murton J,Davies M C R. Soft-sediment deformation during thawing of ice-rich frozen soils:results of scaled centrifuge modelling experiments[J]. Sedimentology,2000,47(3):687-700.
[29]钟建华,王冠民,王夕宾,等.黄河下游冰成滑塌与塌陷构造的研究[J].沉积学报,2002,20(2):261-266.[Zhong Jianhua,Wang Guanmin,Wang Xibin,et al. Study on the ice-induced slump and subsidence structures in the lower course of Yellow River[J]. Acta Sedimentologica Sinica,2002,20(2):261-266.]
[30] Weaver L,Arnaud E. Polyphase glacigenic deformation in the Waterloo Moraine,Kitchener,Ontario,Canada[J]. Sedimentary Geology,2011,235(3/4):292-303.
[31] Moretti M,Soria J M,Alfaro P,et al. Asymmetrical soft-sediment deformation structures triggered by rapid sedimentation in turbiditic deposits(Late Miocene,Guadix Basin,Southern Spain)[J]. Facies,2001,44(1):283-294.
[32] P7ldsaar K,Ainsaar L. Extensive soft-sediment deformation structures in the early Darriwilian(Middle Ordovician)shallow marine siliciclastic sediments formed on the Baltoscandian carbonate ramp,northwestern Estonia[J]. Marine Geology,2014,356:111-127.
[33]刘金华,吴立峰,乔力,等.苏北盆地高邮凹陷深凹带古近系戴南组软沉积物变形构造及沉积模式研究[J].地质论评,2014,60(5):1019-1025.[Liu Jinhua,Wu Lifeng,Qiao Li,et al. Depositional model and characteristic of soft-sediment deformation structures of the Paleogene Dainan Formation in Gaoyou sag,North Jiangsu Basin[J]. Geological Review,2014,60(5):1019-1025.]
[34]杜远生,余文超.地震和非地震引发的软沉积物变形[J].古地理学报,2017,19(1):65-72.[Du Yuansheng,Yu Wenchao.Earthquake-caused and non-earthquake-caused soft-sediment deformations[J]. Journal of Palaeogeography,2017,19(1):65-72.]
[35]山穆玕,著.冯增昭,刘敏,译.地震岩问题[J].古地理学报,2017,19(1):19-64.[Shanmugam G. Feng Zengzhao,Liu Min,Trans. The seismite problem[J]. Journal of Palaeogeography,2017,19(1):19-64.]
[36] Owen G,Moretti M,Alfaro P. Recognising triggers for soft-sediment deformation:current understanding and future directions[J].Sedimentary Geology,2011,235(3/4):133-140.
[37] Shanmugam G. Global case studies of soft-sediment deformation structures(SSDS):definitions,classifications,advances,origins,and problems[J]. Journal of Palaeogeography,2017,6(4):251-320.
[38] Seilacher A. Fault-graded beds interpreted as seismites[J]. Sedimentology,1969,13(1/2):155-159.
[39] Owen G. Experimental soft-sediment deformation:structures formed by the liquefaction of unconsolidated sands and some ancient examples[J]. Sedimentology,1996,43(2):279-293.
[40]冯先岳.地震振动液化形变的研究[J].内陆地震,1989,3(4):299-307.[Feng Xianyue. Study on the deformation caused by seismic vibrational liquefaction[J]. Inland Earthquake,1989,3(4):299-307.]
[41] Moretti M,Alfaro P,Caselles O,et al. Modelling seismites with a digital shaking table[J]. Tectonophysics,1999,304(4):369-383.
[42]鄢继华,崔永北,陈世悦.几种常见震积岩相标志在模拟实验中的识别[J].沉积学报,2009,27(6):1131-1137.[Yan Jihua,Cui Yongbei,Chen Shiyue. Identification of common facies indicators of seismites in simulated experiments[J]. Acta Sedimentologica Sinica,2009,27(6):1131-1137.]
[43]张斌,王萍,王建存.岷江上游堰塞湖沉积中软沉积物变形构造成因讨论[J].地震研究,2011,34(1):67-74.[Zhang Bin,Wang Ping,Wang Jiancun. Discussion of the origin of the soft-sediment deformation structures in Paleo-dammed Lake sediments in the upper reaches of the Minjiang River[J]. Journal of Seismological Research,2011,34(1):67-74.]
[44]冯增昭,鲍志东,郑秀娟,等.中国软沉积物变形构造及地震岩研究简评[J].古地理学报,2017,19(1):7-12.[Feng Zengzhao,Bao Zhidong,Zheng Xiujuan,et al. Researches of soft-sediment deformation structures and seismites in China:a brief review[J]. Journal of Palaeogeography,2017,19(1):7-12.]
[45]冯增昭.一次成功的专题研讨会:“多成因的软沉积物变形构造及地震岩”[J].古地理学报,2017,19(1):1-6.[Feng Zengzhao. A successful symposium of“Multi-origin of soft-sediment deformation structures and seismites”[J]. Journal of Palaeogeography,2017,19(1):1-6.]
[46]李勇,钟建华,邵珠福,等.软沉积变形构造的分类和形成机制研究[J].地质论评,2012,58(5):829-838.[Li Yong,Zhong Jianhua,Shao Zhufu,et al. An overview on the classification and genesis of soft-sediment deformation structure[J]. Geological Review,2012,58(5):829-838.]
[47]栾光忠,李安龙,王建,等.青岛主要海岛成因分类及其地质环境分析[J].中国海洋大学学报,2010,40(8):111-116.[Luan Guangzhong,Li Anlong,Wang Jian,et al. The geological origin division of the main sea island in Qingdao area and environment analysis[J]. Periodical of Ocean University of China,2010,40(8):111-116.]
[48]山东省第四地质矿产勘察院.山东省区域地质[M].济南:山东省地图出版社,2003:1-970.[Shandong Province NO. 4 Institute of Geological and Mineral Survey. Regional geology of Shandong province[M]. Jinan:Shandong Cartographic Press,2013:1-970.]
[49]吕洪波,张海春,王俊,等.山东胶南灵山岛晚中生代浊积岩中发现巨大滑积岩块[J].地质论评,2012,58(1):80-81.[LüHongbo,Zhang Haichun,Wang Jun,et al. The huge slide block is found in Late Mesozoic turbidite in Lingshan Island, Jiaonan,Shandong[J]. Geological Review,2012,58(1):80-81.]
[50]张海春,吕洪波,李建国,等.山东青岛早白垩世新地层单位—灵山岛组[J].地层学杂志,2013,37(2):216-222.[Zhang Haichun,LüHongbo,Li Jianguo,et al. The Lingshandao Formation:a new lithostratigraphic unit of the Early Cretaceous in Qingdao,Shandong,China[J]. Journal of Stratigraphy,2013,37(2):216-222.]
[51]周瑶琪,张振凯,梁文栋,等.山东东部晚中生代构造—岩浆活动及原型盆地恢复[J].地学前缘,2015,22(1):137-156.[Zhou Yaoqi,Zhang Zhenkai,Liang Wendong,et al. Late Mesozoic tectono-magmatic activities and prototype basin restoration in eastern Shandong province,China[J]. Earth Science Frontiers,2015,22(1):137-156.]
[52] Alsop G I,Marco S. Soft-sediment deformation within seismogenic slumps of the Dead Sea Basin[J]. Journal of Structural Geology,2011,33(4):433-457.
[53]董晓朋,吕洪波,张星,等.山东灵山岛早白垩世复理石软沉积物变形期次解析[J].地质论评,2013,59(6):1060-1067.[Dong Xiaopeng,LüHongbo,Zhang Xing,et al. Stage analysis on the soft-sediment deformation in the Early Cretaceous Flysch,Lingshan Island, Shandong province[J]. Geological Review,2013,59(6):1060-1067.]
[54] van Loon A J,Wiggers A J. Metasedimentary“graben”and associated structures in the lagoonal Almere Member(Groningen Formation,The Netherlands)[J]. Sedimentary Geology,1976,16(4):237-254.
[55]张邦花,田洪水,张增奇,等.地质名山馒头山及其附近早寒武世古地震沉积事件研究[J].沉积学报,2012,30(6):1021-1031.[Zhang Banghua,Tian Hongshui,Zhang Zengqi,et al. Paleoseismic depositional events of the famous geological mountainMantoushan and its vicinity in the Early Cambrian[J]. Acta Sedimentologica Sinica,2012,30(6):1021-1031.]
[56] Yang R C,Van Loon A J. Early Cretaceous slumps and turbidites with peculiar soft-sediment deformation structures on Lingshan Island(Qingdao,China)indicating a tensional tectonic regime[J].Journal of Asian Earth Sciences,2016,129:206-219.
[57]杜芳鹏,刘池洋,王建强,等.鄂尔多斯盆地南部上三叠统延长组软沉积变形特征及构造意义[J].现代地质,2014,28(2):314-320.[Du Fangpeng,Liu Chiyang,Wang Jianqiang,et al.Characteristics and tectonic sense of soft sedimentary structures in Yanchang Formation,South Ordos Basin[J]. Geoscience,2014,28(2):314-320.]
[58]邵珠福,钟建华,李勇,等.青岛灵山岛晚中生代重力流沉积特征及环境分析[J].地质论评,2014,60(3):555-566.[Shao Zhufu,Zhong Jianhua,Li Yong,et al. The sedimentary characteristics and environmental analysis of Late Mesozoic gravity flows in Lingshan Island[J]. Geological Review,2014,60(3):555-566.]
[59]张传恒,刘典波,张传林,等.新疆博格达地区早二叠世软沉积物变形构造:弧后碰撞前陆盆地地震记录[J].地学前缘,2006,13(4):255-266.[Zhang Chuanheng,Liu Dianbo,Zhang Chuanlin,et al. Early Permian seismically induced soft-sediment deformational structures in Bogda region,Xinjiang:stratigraphic records of earthquakes in the retroarc collisional foreland basin[J].Earth Science Frontiers,2006,13(4):255-266.]
[60]钟建华,倪良田,邵珠福,等.几种较特殊的地震成因软变形沉积构造[J].地质科学,2015,50(3):665-683.[Zhong Jianhua,Ni Liangtian,Shao Zhufu,et al. Study on several special sedimentary structures of earthquake-induced soft deformations[J]. Chinese Journal of Geology,2015,50(3):665-683.]
[61] Owen G. Load structures:gravity-driven sediment mobilization in the shallow subsurface[J]. Geological Society,London,Special Publications,2003,216(1):21-34.
[62]乔秀夫,李海兵.枕、球—枕构造:地层中的古地震记录[J].地质论评,2008,54(6):721-730.[Qiao Xiufu,Li Haibing. Pillow,ball-and-pillow structures:paleo-seismic records within strata[J].Geological Review,2008,54(6):721-730.]
[63] Yamamoto Y. Dewatering structure and soft-sediment deformation controlled by slope instability:examples from the Late Miocene to Pliocene Miura-Boso accretionary prism and trench-slope basin,central Japan[J]. Marine Geology,2014,356:65-70.
[64]杨剑萍,聂玲玲,杨君.柴达木盆地西南缘新近系与地震沉积有关的软沉积物变形构造及其地质意义[J].沉积学报,2008,26(6):967-974.[Yang Jianping,Nie Lingling,Yang Jun. Softsediment deformation structures of Neogene related to earthquake and its geological significance in the southwestern margin of Qaidam Basin[J]. Acta Sedimentologica Sinica,2008,26(6):967-974.]
[65] Finkl Jr C W. Sedimentary structures—their character and physical basis:J.R.L. Allen,1982. Vols. I,II. Developments in Sedimentology,30A and 30B. Elsevier,Amsterdam,Vol. I:xvii+593pp.,US$98.00,Dfl.245.00; Vol. II:xiii+663 pp.,US$104.00,Dfl.260.00[J]. Earth-Science Reviews,1983,19(4):362-363.
[66]周瑶琪,张振凯,许红,等.灵山岛沉积物软变形构造特征[J].海洋地质前沿,2015,31(4):42-54.[Zhou Yaoqi,Zhang Zhenkai,Xu Hong,et al. Soft-sediment deformation structures in the sediments at Lingshan Island[J]. Marine Geology Frontiers,2015,31(4):42-54.]
[67] Simms M J. Uniquely extensive soft-sediment deformation in the Rhaetian of the UK:evidence for earthquake or impact?[J].Palaeogeography,Palaeoclimatology, Palaeoecology,2007,244(1/2/3/4):407-423.
[68]乔秀夫,宋天锐,高林志,等.碳酸盐岩振动液化地震序列[J].地质学报,1994,68(1):16-34.[Qiao Xiufu,Song Tianrui,Gao Linzhi,et al. Seismic sequence in carbonate rocks by vibrational liquefaction[J]. Acta Geologica Sinica,1994,68(1):16-34.]
[69]钟建华,梁刚.沉积构造的研究现状及发展趋势[J].地质论评,2009,55(6):831-839.[Zhong Jianhua,Liang Gang. Situation of study and development tendency of sedimentary structure[J].Geological Review,2009,55(6):831-839.]
[70] Mc Laughlin P I,Brett C E. Eustatic and tectonic control on the distribution of marine seismites:examples from the Upper Ordovician of Kentucky,USA[J]. Sedimentary Geology,2004,168(3/4):165-192.
[71] Rossetti D F,Santos Jr A E. Events of sediment deformation and mass failure in Upper Cretaceous estuarine deposits(CametáBasin,northern Brazil)as evidence for seismic activity[J]. Sedimentary Geology,2003,161(1/2):107-130.
[72]周勇,纪友亮,万璐,等.山东省胶莱盆地东北部下白垩统莱阳组震积岩特征及地质意义[J].古地理学报,2011,13(5):517-528.[Zhou Yong,Ji Youliang,Wan Lu,et al. Characteristics and geologic significance of seismites in the Lower Cretaceous Laiyang Formation in northeastern Jiaolai Basin in Shandong province[J].Journal of Palaeogeography,2011,13(5):517-528.]
[73]刘颖,谢君斐.砂土震动液化[M].北京:地震出版社,1984:1-255.[Liu Ying,Xie Junfei. Sand vibration liquefaction[M]. Beijing:Seismological Press,1984:1-255.]